DOCSLIB.ORG

Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 8-1977 Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan Norman A. Lovan Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Lovan, Norman A., "Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan" (1977). Master's Theses. 2207. https://scholarworks.wmich.edu/masters_theses/2207 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. ANALYSIS OF AN INTERLOBATE BOUNDARY IN THE WISCONSINAN DRIFT OF KALAMAZOO COUNTY AND ADJACENT AREAS IN SOUTHWESTERN MICHIGAN by Norman A. Lovan A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the Degree of Master of Science Western Michigan University Kalamazoo, Michigan August 19 77 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ANALYSIS OF AN INTERLOBATE BOUNDARY IN THE WISCONSINAN DRIFT OF KALAMAZOO COUNTY AND ADJACENT AREAS IN SOUTHWESTERN MICHIGAN Norman A. Lovan, M.S. Western Michigan University, 1977 ABSTRACT A detailed investigation of selected textural and mineralogical aspects of tills in southwestern Michigan is used to define an interlobate boundary relationship be­ tween the Wisconsinan ice of the Lake Michigan and Saginaw lobes. Bedrock underlying the study area contributed lit­ tle to the bulk composition of the tills investigated. However, morainal development in the study area shows strong correlation with bedrock topography. In a discussion of the deglaciation of Michigan and the study area, a history of morainal development is re­ viewed and attention is focused on the reentrant district located in Kalamazoo and neighboring counties. Attempts to delineate t i l l s of the Lake Michigan and Saginaw lobes using textural and magnetic susceptibility data were in­ conclusive. However, the character and extent of an in ­ terlobate boundary relationship in the study area is de­ limited by ratios of heavy minerals, as well as, ratios of the 7A/10A peaks produced by clays in X-ray diffractograms. i i Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ACKNOWLEDGEMENTS I wish to extend my sincere thanks to Dr. W. Thomas Straw who suggested this problem and encouragingly direct­ ed my efforts during the course of the study. My thanks also go to Drs. Lloyd Schmaltz, W. David Kuenzi, and Cas­ par Cronk for their suggestions and review of the manu­ script. Appreciation need also be expressed to Dr. W. B. Harrison of Western Michigan U niversity's Geology Depart­ ment for suggestions and aid during sample preparation and to Dr. Stoline of W.M.U.’s Mathematics Department for aid in the statistical analysis of my data. Additionally, I extend my appreciation to my fellow graduate students, es­ pecially Robert Kell, Hall Taylor, Jonathan "Nate” Fuller, and Warren P. French for th e ir continuous moral support and criticism and to Bob Havira of Western Michigan Uni­ v e rs ity 's Geology Department for photographic work. To Indiana University, Bloomington, Indiana, and Dr. J. Mead I express my thanks for the use of their magnetic susceptibility bridge. Also, to Dr. Ned Bleuer of the Indiana Geological Survey I extend my appreciation for suggestions on sample analysis and aid while at Indiana University. During the first two years of my study I was the re­ cipient of Graduate Fellowships funded by Western Michigan University's Graduate College and the Department of Geo- i i i Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. i v logy. Additionally, I received a research grant funded by the Graduate College. Finally, I wish to express my gratitude to Linda Lovan for her continued encouragement, to my parents, Paul and Mary Lou Lovan, a special appreciation for the financial and moral aid in what seemed like a c r is is , and to Janell B. Smith for her assistance in the typing and preparation of the manuscript, as well as, her personal friendship. To all these people and many others I extend my thanks. *"*' Norman A. Lovan Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page{s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find ja good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from (eft to right in equal sections with a small overlap. If necessary, sectioning is continued again — beginning below the first row and continuing on until complete. 4. The majority of users indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. Silver prints of "photographs" may be ordered at additional charge by writing the Order Department, giving the catalog number, title, author and specific pages you wish reproduced. 5. PLEASE NOTE: Some pages may have indistinct print. Filmed as received. University Microfilms International 300 North Zeeb Road Ann Arbor, Michigan 48106 USA St. John's Road, Tyler's Green High Wycombe, Bucks, England HP10 8HR Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. MASTERS THESIS 13^10,287 LOVAN, Norman Alan ANALYSIS OF AN INTERLOBATE BOUNDARY IN THE WISCONSINAN DRIFT OF KALAMAZOO COUNTY AND ADJACENT AREAS IN SOUTHWESTERN MICHIGAN. Western Michigan University, M.S., 1977 Geology Xerox University Microfiims,Ann Arbor, Michigan 48106 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS PAGE A b s t r a c t ..................................................................................................... i i Acknowledgements .................................................................................. i i i Table of contents ............................................................................. v List of figures ....................................................................................... v ii L ist of t a b l e s ....................................................................................... x Introduction ........................................................................................... 1 Bedrock geology .................................................................................. 4 Glacial geology .................................................................................. 6 Introduction ....................................................................................... 6 Till classification ................................................................... 12 Deglaciation of Michigan .......................................................... 17 Terminal and lateral moraines in the study area . 22 Valparaiso morainic system ................................................ 22 Kendall moraine ........................................................................ 24 Kalamazoo morainic system ................................................ 27 Tekonsha-morainic system ..................................................... 29 L o c a tio n ..................................................................................................... 30 T ech n iq u es ................................................................................................ 31 Field sampling .................................................................................. 31 Laboratory analysis ................................................................... 32 Analysis of an interlobate boundary .................................. 35 Textural analysis ........................................................................ 37 v Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PAGE Magnetic susceptibility analysis ....................................... 45 Heavy mineral analysis .............................................................
Load more

Recommended publications
  • Lexicon of Pleistocene Stratigraphic Units of Wisconsin
    Lexicon of Pleistocene Stratigraphic Units of Wisconsin ON ATI RM FO K CREE MILLER 0 20 40 mi Douglas Member 0 50 km Lake ? Crab Member EDITORS C O Kent M. Syverson P P Florence Member E R Lee Clayton F Wildcat A Lake ? L L Member Nashville Member John W. Attig M S r ik be a F m n O r e R e TRADE RIVER M a M A T b David M. Mickelson e I O N FM k Pokegama m a e L r Creek Mbr M n e M b f a e f lv m m i Sy e l M Prairie b C e in Farm r r sk er e o emb lv P Member M i S ill S L rr L e A M Middle F Edgar ER M Inlet HOLY HILL V F Mbr RI Member FM Bakerville MARATHON Liberty Grove M Member FM F r Member e E b m E e PIERCE N M Two Rivers Member FM Keene U re PIERCE A o nm Hersey Member W le FM G Member E Branch River Member Kinnickinnic K H HOLY HILL Member r B Chilton e FM O Kirby Lake b IG Mbr Boundaries Member m L F e L M A Y Formation T s S F r M e H d l Member H a I o V r L i c Explanation o L n M Area of sediment deposited F e m during last part of Wisconsin O b er Glaciation, between about R 35,000 and 11,000 years M A Ozaukee before present.
    [Show full text]
  • Stratigraphy of Lake Michigan Lobe Deposits in Van Buren County, Michigan
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 6-2003 Stratigraphy of Lake Michigan Lobe Deposits in Van Buren County, Michigan Steven P. Beukema Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Beukema, Steven P., "Stratigraphy of Lake Michigan Lobe Deposits in Van Buren County, Michigan" (2003). Master's Theses. 4445. https://scholarworks.wmich.edu/masters_theses/4445 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. f STRATIGRAPHY OF LAKE MICiflGANLOBE DEPOSITS IN VAN BUREN COUNTY, MICiflGAN by Steven P. Beukema A Thesis Submitted to the Facultyof The Graduate College in partial fulfillmentof the requirements forthe Degree of Master of Science Departmentof Geosciences WesternMichigan University Kalamazoo, Michigan June 2003 Copyright by Steven P. Beukema 2003 ACKNOWLEDGMENTS There are several people who deserve recognition for their generous support. I would first like to thank Bill Bush forsuggesting the idea of doing graduate work in geology at WMU. Two of my cohorts in the department, Andrew Kozlowski and Brian Bird, deserve special recognition for endless hours of ruminating with me about many things, in particular about the last 20,000 years in southwest Michigan. I wish also to thank Andrew forstepping out of his pessimistic outlook to offerme continual encouragement to pursue science and academia. Brian was always willing to spend time making figures and answering my constant questions about GIS, Canvas, and a host of other programs.
    [Show full text]
  • Geologic Resources Inventory Map Document for Indiana Dunes National Lakeshore
    U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Indiana Dunes National Lakeshore GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Indiana Dunes National Lakeshore indu_geology.pdf Version: 3/4/2014 I Indiana Dunes National Lakeshore Geologic Resources Inventory Map Document for Indiana Dunes National Lakeshore Table of Contents Geologic R.e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .M...a..p.. .D..o..c..u..m...e..n..t....................................................................... 1 About the N..P..S.. .G...e..o..l.o..g..i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .P...r.o..g..r.a..m........................................................... 2 GRI Digital .M...a..p.. .a..n..d.. .S..o..u..r.c..e.. .M...a..p.. .C..i.t.a..t.i.o..n............................................................................... 4 Map Unit Li.s..t.......................................................................................................................... 5 Map Unit De..s..c..r.i.p..t.i.o..n..s............................................................................................................. 7 Qlmm - Fille..d.. .a..n..d.. .m..o..d..i.f.i.e..d../.d..i.s..t.u..r.b..e..d.. .l.a..n..d.. .(.H..o..l.o..c..e..n..e..).................................................................................................. 7 Qlma1 - Ch.a..n..n..e..l. .a..n..d.. .f.l.o..o..d..p..l.a..in.. .(..H..o..l.o..c..e..n..e..)................................................................................................................. 7 Qlma2 - Ch.a..n..n..e..l. .a..n..d.. .f.l.o..o..d..p..l.a..in.
    [Show full text]
  • Behavior of the James Lobe, South Dakota During Termination I
    Behavior of the James Lobe, South Dakota during Termination I A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in the Department of Geology of the McMicken College of Arts and Sciences by Stephanie L. Heath MSc., University of Maine BSc., University of Maine July 18, 2019 Dissertation Committee: Dr. Thomas V. Lowell Dr. Aaron Diefendorf Dr. Aaron Putnam Dr. Dylan Ward i ABSTRACT The Laurentide Ice Sheet was the largest ice sheet of the last glacial period that terminated in an extensive terrestrial margin. This dissertation aims to assess the possible linkages between the behavior of the southern Laurentide margin and sea surface temperature in the adjacent North Atlantic Ocean. Toward this end, a new chronology for the westernmost lobe of the Southern Laurentide is developed and compared to the existing paradigm of southern Laurentide behavior during the last glacial period. Heath et al., (2018) address the question of whether the terrestrial lobes of the southern Laurentide Ice Sheet margin advanced during periods of decreased sea surface temperature in the North Atlantic. This study establishes the pattern of asynchronous behavior between eastern and western sectors of the southern Laurentide margin and identifies a chronologic gap in the western sector. This is the first comprehensive review of the southern Laurentide margin since Denton and Hughes (1981) and Mickelson and Colgan (2003). The results of Heath et al., (2018) also revealed the lack of chronologic data from the Lobe, South Dakota, the westernmost lobe of the southern Laurentide margin.
    [Show full text]
  • Stratigraphic Analysis of Diamicton Units in Southern Allegan County, Michigan
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 4-2002 Stratigraphic Analysis of Diamicton Units in Southern Allegan County, Michigan Shannon A. Wong Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Wong, Shannon A., "Stratigraphic Analysis of Diamicton Units in Southern Allegan County, Michigan" (2002). Master's Theses. 4417. https://scholarworks.wmich.edu/masters_theses/4417 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. STRATIGRAPHIC ANALYSIS OF DIAMICTON UNITS IN SOUTHERN ALLEGAN COUNTY, MICHIGAN by Shannon A. Wong A Thesis Submitted to the Faculty of The Graduate College in partial fulfillmentof the requirements for the Degree of Master of Science Department of Geosciences WesternMichigan University Kalamazoo, Michigan April 2002 Copyright by Shannon A. Wong 2002 ACKNOWLEDGMENTS I gratefullyacknowledge some of the geology graduate students at Western Michigan University and friendswho have accompanied me in the field. Their assistance is greatly appreciated. I would like to thank John Grace, Andrew Kozlowski, and Brian Bird for their advice and support at the onset of my laboratory work. Getting started is the hardest part, especially when learning a new technique. I would like to acknowledge the US Army Research Officefor one year of sup­ port. I would also like to acknowledge my main advisor, Alan Kehew, forhis tremen­ dous help on my thesis and Ron Chase forintroducing me to his research site in Allegan County.
    [Show full text]
  • PLEISTOCENE STRATIGRAPHIC UNITS of Wisconsin
    MISCELLANEOUS PAPER 84-1 PLEISTOCENE STRATIGRAPHIC UNITS OF WISCONSiN by David M. Mickelson, Lee Clayton, Robert W. Baker, William N. Mode and Allan F. Schneider available from Geological and Natural History Survey University of Wisconsin-Extension 1815 University Avenue Madison, Wisconsin 53705 MISCELLANEOUS PAPER 84-1 PLEISTOCENE STRATIGRAPHIC UNITS OF WISCONSIN by David M. Mickelson, Lee Clayton, Robert W. Baker, William N. Mode and Allan F. Schneider available from Geological and Natural History Survey University of Wisconsin�Extension 1815 University Avenue Madison, Wisconsin 53705 JUL 1984 CONTENTS Acknowledgements ..................... ..............It ................................................It .................. iv Abstract ............................................................................................................................ I Introduction It .. .. ........ .. .... .. ................ .. ........ .. .. .. ........ .. .. .. .. .. .... ........ .. .... .. .. ............ .. ........ I Principles of Lithostratigraphic Classification in Wisconsin •• •••••••• 2 Summary of Lithostratigraphic Units Defined in this Paper ••••••••••••• 5 Units of Probable Pre-Wisconsinan and Early Wisconsinan Age •••••••• 5 Units of Late Wisconsinan Age ............................................................................ 7 References Cited ............................................................................................................ 12 Appendix 1. Walworth Formation .. ................ ......It .... ....It
    [Show full text]
  • Glacial Lakes Around Michigan
    The Glacial Lakes around Michigan By William R. Farrand, University of Michigan Bulletin 4, revised 1988 Geological Survey Division Michigan Department of Environmental Quality Bulletin 4 - Glacial Lakes Around Michigan By William R. Farrand, University of Michigan, 1967 revised 1998 Illustrated by Kathline Clahassey, University of Michigan Published by Michigan Department of Environmental Quality. Geological Survey Division Contents Preface............................................................................................................................................ 3 Abstract........................................................................................................................................... 3 Introduction ..................................................................................................................................... 4 Was There A Glacier?..................................................................................................................... 4 Figure 1: The modem Great Lakes have a water surface area greater than 95,000 square miles, a total drainage area of about 295,000 square miles, and a shore line 8,300 miles long. ................................................................................................4 Figure 2: Features originating at a glacier front occur in a definite order. ...................................................................................5 Figure 3: Landforms of continental glaciation are unmistakable. Compare with figure 2 ............................................................5
    [Show full text]
  • Proceedings of the Indiana Academy Of
    The Tinley Moraine in Indiana 1 Allan F. Schneider, Indiana Geological Survey Abstract The Tinley Moraine, which was named in Illinois for a subsidiary ridge behind the main part of the Valparaiso Morainic System, has received little recognition as a discrete moraine in Indiana. Recent mapping sug- gests, however, that ice of the Lake Michigan Lobe probably did recede some unknown distance from its position along the Valparaiso Moraine and then readvanced to form the Tinley Moraine. The Tinley Moraine enters Indiana in west-central Lake County, and its main ridge can be traced for about 20 miles across Lake County and western Porter County. It is more readily recognized as a discrete moraine by ice-block depressions and drainage relations along its distal margin than by its height or good internal morphology. The crest of the Tinley ridge gradually decreases in elevation from 736 feet at the state line to about 700 feet at the eastern end of the segment, where the moraine be- comes obscure near a prominent gap in the Valparaiso Moraine. Here the terminal zone of the Tinley ice apparently curved northward through an arc of about 90 degrees and is represented by an upland till plain that was probably deposited with the ice front standing in a lake. Farther north- east the terminal zone of the ice possibly is marked by an undulating till belt that trends eastward through northeastern Porter County and northeastward through northwestern LaPorte County. This belt has long been considered to be part of the Lake Border Morainic System, which is, however, presumably younger than the Tinley Moraine.
    [Show full text]
  • Guide Leaflet, Geological Science Field Trip, Palos Hills
    G#£i SuJ^OLxJ GUIDE LEAFLET 1971 G Reprinted in 1981 PALOS HILLS AREA GEOLOGICAL SCIENCE FIELD TRIP November 12, 1971 Cook and Du Page Counties Palos Park and Sag Bridge 7.5-Minute Quadrangles ^ <*& v^Vv ,o wov David L. Reinertsen Dwain J. Berggren Leaders Illinois Institute of Natural Resources, State Geological Survey Division, Champaign, Illinois 61820 SURVEY ILLINOIS »T»Te0t0LOOICAL 3 3051 00006 9470 . PALOS HILLS GEOLOGICAL SCIENCE FIELD TRIP ITINERARY Line up on West 97th Street at Roberts Road, opposite H. H. Conrady Junior High School, heading west. 0.0 0.0 Turn right (north) on Roberts Road (30th Avenue). We are driving along the Tinley Moraine, a wide belt of gravel and earth ridges that form the higher hills in the Hickory Hills Golf Course west of the road. This belt of ridges is as much as 6 miles wide, and it extends roughly parallel to Lake Michigan and almost continuously from Wisconsin to Indiana. The Tinley Moraine was deposited about 14,000 years ago by a glacier flowing from Canada into Illinois through the trough that now contains Lake Michigan. As the glacier melted, water was trapped between the Tinley Moraine and the ice front. As the ice front melted back into the Lake Michigan basin, a large lake came into being, covering all the land east of the Tinley Moraine. The place covered by the glacial lake--the area that was the lake bed--is called the Chicago Lake Plain. The Chicago Lake Plain is an extremely flat region about 45 miles long and 15 miles wide, bounded on the west by the Tinley Moraine and containing the city of Chicago and many of its suburbs (see figure 1) The lake that formed between the Tinley Moraine and the glacier is called Lake Chicago, and it lasted almost 4,000 years (from about 14,000 years up to about 10,500 years before present) at levels fluctuating between approximately 640 feet and 590 feet MSL (feet above mean sea level).
    [Show full text]
  • Geology of the Chicago Region
    STATE OF ILLINOIS WILLIAM G. STRATTON, GoHntor DEPARTMENT OP REGISTRATION AND EDUCA'l'ION VERA M. BINKS, Dj,«UJr DIVISION OP THE STATE GEOLOG ICAL SURVEY M. M. LEIGHTON, Cbl;J URBANA B U L L E T I N N 0 . 65, P A 1t T I I GEOLOGY OF THE CHICAGO REGION PART II-IBEPLEISTOCENE BY J llARLBN BRETZ Pll.INTED BYUTHOlllTY A OF THE STATE O"l' lLLlNOlS URBANA, ILLINOIS 1955 STATE OF ILLINOIS WILLIAM G. STRATTON, Governor DEPARTMENT OF REGISTRATION AND EDUCATION VERA M. BINKS, Director DIVISION OF THE STATE GEOLOG IC AL SURVEY M. M. LEIGHTON, Chief URBANA B u L L E T I N N 0 . 65, p A RT I I GEOLOGY OF THE CHICAGO REGION PART II - THE PLEISTOCEN E BY J HARLEN BRETZ PRINTED BY AUTHORITY OF THE STATE OF ILLINOIS URBANA, ILLINOIS 1955 ORGANIZATION ST ATE OF ILLINOIS HON. WILLIAM G. STRATTON, Governor DEPARTMENT OF REGISTRATION AND EDUCATION HON. VERA M. BINKS, Director BOARD OF NATURAL RESOURC ES AND CONS ERVAT IO N HON. VERA M. BINKS, Chairman W. H. NEWHOUSE, PH.D., Geology ROGER ADAMS, PH.D., D.Sc., Chemistry R. H. ANDERSON, B.S., Engineering 0 A. E. EMERSO�. PH.D., Biology LEWIS H. TIFFANY, PH.D., Po.D., Forestry W. L. EVERITT, E.E., PH.D., Representing the President of the University of Illinois DELYTE W. MORRIS, PH.D. President of Southern Illinois University GEOLOGICAL SURVEY DIVIS IO N M. M. LEIGHTON, PH.D., Chief STATE GEOLOGICAL SURVEY DIVISION Natural Resources Building, Urbana M. M. LEIGHTON, PH.D., Chief Esm TOWNLEY, M.S., Geologist and Assistant to the Chief VELDA A.
    [Show full text]
  • Glaciotectonic Deformation Along the Valparaiso Upland in Southwest Michigan, USA
    Western Michigan University ScholarWorks at WMU Dissertations Graduate College 6-2010 Glaciotectonic Deformation along the Valparaiso Upland in Southwest Michigan, USA Brian C. Bird Western Michigan University Follow this and additional works at: https://scholarworks.wmich.edu/dissertations Part of the Geology Commons, Geomorphology Commons, and the Glaciology Commons Recommended Citation Bird, Brian C., "Glaciotectonic Deformation along the Valparaiso Upland in Southwest Michigan, USA" (2010). Dissertations. 349. https://scholarworks.wmich.edu/dissertations/349 This Dissertation-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Dissertations by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. GLACIOTECTONIC DEFORMATION ALONG THE VALPARAISO UPLAND IN SOUTHWEST MICHIGAN, USA by Brian C. Bird A Dissertation Submitted to the Faculty of The Graduate College in partial fulfillment of the requirements for the Degree of Doctor of Philosophy Department of Geoscience Advisor: Alan E. Kehew, Ph.D. Western Michigan University Kalamazoo, Michigan June 2010 UMI Number: 3470399 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMI' Dissertation Publishing UMI 3470399 Copyright 2010 by ProQuest LLC, All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code.
    [Show full text]
  • Chicagoland Geology and the Making of a Metropolis
    Chicagoland Geology and the Making of a Metropolis Field Excursion for the 2005 Annual Meeting Association of American State Geologists June 15, 2005 Michael J. Chrzastowski Open File Series OFS 2005-9 Rod R. Blagojevich, Governor Illinois Department of Natural Resources Joel Brunsvold, Director ILLINOIS STATE GEOLOGICAL SURVEY William W. Shilts, Chief 97th Annual Meeting St. Charles Illinois AASG Sponsors The Illinois State Geological Survey and the Association of American State Geologists gratefully acknowledge the generous support of the following organizations and individuals as sponsors of the 2005 Annual Meeting in St. Charles, Illinois. Diamond Sponsors ($5,000 or more) Isotech Laboratories, Champaign, Illinois (Dennis D. Coleman, President and Laboratory Director) Preston Exploration (Arthur F. Preston) Gold Sponsors ($1,000 or more) Bi-Petro (John F. Homeier, President) Illinois Oil and Gas Association William F. Newton Podolsky Oil Company (Bernard Podolsky, President) U.S. Silica Company Silver Sponsors ($500 or more) Anonymous James S. and Barbara C. Kahn Shabica and Associates (Charles Shabica) Excursion Bus Hosts Michael J. Chrzastowski Daniel J. Adomaitis Chicagoland Geology and the Making of a Metropolis Field Excursion for the 2005 Annual Meeting Association of American State Geologists June 15, 2005 Michael J. Chrzastowski Rod R. Blagojevich, Governor Illinois Department of Natural Resources Joel Brunsvold, Director ILLINOIS STATE GEOLOGICAL SURVEY William W. Shilts, Chief 615 East Peabody Drive Champaign, Illinois 61820-6964 217-244-2414 www.isgs.uiuc.edu “Make no little plans; they have no magic to stir men’s blood and probably themselves will not be realized. Make big plans; aim high in hope and work.” Daniel Hudson Burnham (1846–1912) Architect for the 1893 World’s Columbian Exposition held at Chicago and lead author of the 1909 Plan of Chicago.
    [Show full text]